1. |
Komodo
03:32
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i dont know what i could do (i dont know
i dont know what i should do (i dont know
i cant bare to step out side (step outside
i dont care ill stay inside
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2. |
Nervous
03:54
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i can tell you're alone and i see it
run along to the city
put on some nirvana
lets smoke marijuana
i know i know there's a word that's over due
i know i know i know i know
all along i cannot choose
i know i know and i forgot
all the words its all i got
i know i know i know i know
All the stars do fall apart
i cant tell its so cold in the summer
wont be any longer
down with the sickness
see you at the picnic
uh
i know i know there's a word that's over due
i know i know i know i know
all along i cannot choose
i know i know and i forgot
all the words its all i got
i know i know i know i know
All the stars do fall apart
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3. |
Sigh
03:37
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ahhh ohh ahhh uhhhh
soft side
fall into
forfeit
silence to
Few stick
cellophane
step down
you are dead
????
mmmmmm
I
SIGH
SIGH
SIGH
SIGH
SIGH
SIGH
SIGH
SIGH
I found fortitude
???
???
i cant tell
few still
I
SIGH
SIGH
SIGH
SIGH
SIGH
SIGH
SIGH
SIGH
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4. |
Sun was high so was I
02:30
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i went for a walk watched the cars go by
the sun was high
i thought of you
i thought of you
i went for a walk the sun was high
it sure was high, and so was I
So was I
So was i
i sure was high
i thought of you
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5. |
Midtown
01:26
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Bute straddles the divide between highland and lowland Scotland with the Highland Boundary Fault cutting NNE-SSW through the island between Rothesay Bay and Scalpsie Bay. To the north of this line are metamorphosed sandstones and mudstones (i.e. psammites and pelites) which constitute the Southern Highland Group of the Dalradian. To its south are the conglomerates, sandstones, mudstones and siltstones of the Devonian age Stratheden Group (a division of the Old Red Sandstone) and of the Carboniferous age Inverclyde Group. Associated with the latter are Carboniferous extrusive igneous rocks, mainly lavas and tuffs of the Clyde Plateau Volcanic Formation. These occur north of Ascog, northeast of Scalpsie and south of Kilchattan Bay.
The metamorphic rocks of the Dalradian sequence is divided locally into a couple of groups, themselves subdivided into formations, each of which contains ‘members’. The youngest strata are at the top of the list:
Trossachs Group
Ardscalpsie Formation
Quien Hill Grit Member
Loch Dhu Slate Member (includes ‘Rothesay Limestone’)
Southern Highlands Group
St Ninian Formation
Toward Quay Grit Member
Bullrock Greywacke Member
Dunoon Phyllite Formation
The Palaeozoic sedimentary and extrusive igneous sequence in stratigraphic order (i.e. youngest at top) is as follows. All are of Carboniferous age except the Bute Conglomerate, which is late Devonian and separated from the overlying Kinnesswood sandstones and mudstones by an unconformity.
Strathclyde Group
Clyde Plateau Volcanic Formation
Birgidale Mudstone Formation
Inverclyde Group
Clyde Sandstone Formation
Ballagan Formation
Kinnesswood Formation
Stratheden Group
Bute Conglomerate Formation
A couple of thin coal seams are recorded within the volcanic sequence inland of Asco
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6. |
Lazy
02:44
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The Wallowa Ranger Station at 602 W. 1st St. in Wallowa, Oregon is a historic station built in 1936. It was listed on the National Register of Historic Places in 2009; the listing included five contributing buildings. It includes Late 19th and Early 20th Century American Movements architecture and Rustic architecture designed by U.S. Forest Service architects.
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